2020
DOI: 10.1002/mma.6984
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Synchronization of the nonlinear advection‐diffusion‐reaction processes

Abstract: This paper presents a dynamical and generalized synchronization (GS) of two dependent chaotic nonlinear advection‐diffusion‐reaction (ADR) processes with forcing term, which is unidirectionally coupled in the master‐slave configuration. By combining backward differentiation formula‐Spline (BDFS) scheme with the Lyapunov direct method, the GS is studied for designing controller function of the coupled nonlinear ADR equations without any linearization. The GS behaviors of the nonlinear coupled ADR problems are o… Show more

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Cited by 3 publications
(1 citation statement)
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“…In the late 1970 s, Kuramoto [1] and Sivashinsky [2] independently derived the Kuramoto-Sivashinsky (KS) equation and worked on turbulence phenomena in chemistry and thermal diffusive instability in laminar flame fronts. If b = 0, then equation (1) is defined as the KS equation, which is a canonical nonlinear evolution equation with a wide range of applications in modelling various scientific engineering, and physical phenomena, including diffusion and chaos [3][4][5][6] and the flow of thin liquid membranes, reaction diffusion systems [7][8][9][10][11] and stationary solitary pulses in a falling film [12]. This equation can also be used to define long waves in a viscous fluid along an inclined plane [13,14], stress waves in fragmented porous media [15], and unstable drift waves in plasma [16].…”
Section: Introductionmentioning
confidence: 99%
“…In the late 1970 s, Kuramoto [1] and Sivashinsky [2] independently derived the Kuramoto-Sivashinsky (KS) equation and worked on turbulence phenomena in chemistry and thermal diffusive instability in laminar flame fronts. If b = 0, then equation (1) is defined as the KS equation, which is a canonical nonlinear evolution equation with a wide range of applications in modelling various scientific engineering, and physical phenomena, including diffusion and chaos [3][4][5][6] and the flow of thin liquid membranes, reaction diffusion systems [7][8][9][10][11] and stationary solitary pulses in a falling film [12]. This equation can also be used to define long waves in a viscous fluid along an inclined plane [13,14], stress waves in fragmented porous media [15], and unstable drift waves in plasma [16].…”
Section: Introductionmentioning
confidence: 99%